2011
DOI: 10.3133/sir20115020
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Effects of natural and human factors on groundwater quality of basin-fill aquifers in the southwestern United States: Conceptual models for selected contaminants

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Cited by 8 publications
(16 citation statements)
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“…We therefore suggest that the isotopic data likely reflect use of multiple groundwater systems bearing water that experienced differing degrees of evaporation prior to recharge. Previous work on public supply wells has documented a wide range of recharge modes for groundwaters within this part of the SLV, such as subsurface inflow from mountain blocks, infiltration from mountain‐front streams, and infiltration of excess irrigation and lawn water [ Thiros and Manning , ; Bexfield et al ., ], but not the wide range of isotopic compositions measured here for group 6 tap waters.…”
Section: Discussionmentioning
confidence: 56%
“…We therefore suggest that the isotopic data likely reflect use of multiple groundwater systems bearing water that experienced differing degrees of evaporation prior to recharge. Previous work on public supply wells has documented a wide range of recharge modes for groundwaters within this part of the SLV, such as subsurface inflow from mountain blocks, infiltration from mountain‐front streams, and infiltration of excess irrigation and lawn water [ Thiros and Manning , ; Bexfield et al ., ], but not the wide range of isotopic compositions measured here for group 6 tap waters.…”
Section: Discussionmentioning
confidence: 56%
“…Even though recharge in the West Salt River Valley and Central Valley increased almost sevenfold from predevelopment conditions, discharge increased even more, resulting in large water-level declines in parts of these aquifers Modified from Bexfield and others (19)…”
Section: Principal Aquifermentioning
confidence: 99%
“…Estimated groundwater residence times in the study basins under developed conditionsaffected by artificial recharge and groundwater pumping-are shorter than under predevelopment conditions. (19) As a result, groundwater moves through the aquifer more quickly, potentially transporting contaminants down to the groundwater supply. Geochemical conditions, such as redox and pH, can be altered by oxygen-rich artificial recharge and water-level declines caused by pumping wells.…”
Section: Pumping Changes Natural Groundwater Flow Systemsmentioning
confidence: 99%
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